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  • Late Quaternary sediments and climatic change in Swaziland in Palaeoecology of Africa and the surrounding islands. Volume 15. Southern African Society for Quaternary research. Proceedings.
  • data which show that a long series of conspicuous changes in climate and vegetation occurred over the last 35 000 years. These changes include greater expansions of sub-humid montane, relatively dry savanna and cool ericaceous elements in the Late
  • Lake Malawi levels have been as much as 5 m above modern peak values during the early? Holocene but, until more is known about changes in the overflow, the palaeoclimatic significance of these high levels must remain in doubt. In an attempt to view
  • The physical factors which affected the biological patterns of Africa during the last glacial maximum are discussed. Changes in temperature, humidity and wind force on the continent are discussed in a survey of the evidence on periglacial
  • , possibly related to early Quaternary climatic, tectonic or eustatic changes, has had significant influence on the westward-flowing drainage systems in South West Africa.